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The origin and pre-Cenozoic evolution of the Tibetan Plateau
Different hypotheses have been proposed for the origin and pre-Cenozoic evolution of the
Tibetan Plateau as a result of several collision events between a series of Gondwana …
Tibetan Plateau as a result of several collision events between a series of Gondwana …
Building the Zagros collisional orogen: timing, strain distribution and the dynamics of Arabia/Eurasia plate convergence
The Zagros Mountains are the result of the Arabia/Eurasia collision initiated at~ 35Ma as the
rifted Arabian lithosphere was underthrusted beneath the Iranian plate due to its negative …
rifted Arabian lithosphere was underthrusted beneath the Iranian plate due to its negative …
Continental arc volcanism as the principal driver of icehouse-greenhouse variability
Variations in continental volcanic arc emissions have the potential to control atmospheric
carbon dioxide (CO2) levels and climate change on multimillion-year time scales. Here we …
carbon dioxide (CO2) levels and climate change on multimillion-year time scales. Here we …
[HTML][HTML] Tectonic, magmatic, and metallogenic evolution of the Tethyan orogen: From subduction to collision
This paper reviews the tectonic, magmatic, and metallogenic history of the Tethyan orogen
from the Carpathians to Indochina. Focus is placed on the formation of porphyry Cu±Mo±Au …
from the Carpathians to Indochina. Focus is placed on the formation of porphyry Cu±Mo±Au …
High Sr/Y magmas reflect arc maturity, high magmatic water content, and porphyry Cu±Mo±Au potential: Examples from the Tethyan arcs of central and eastern Iran …
The temporal and geochemical evolution of arc magmatism that culminated in porphyry
Cu±Mo±Au deposit formation has been studied in three separate Neo-Tethyan arc systems …
Cu±Mo±Au deposit formation has been studied in three separate Neo-Tethyan arc systems …
Zircon U–Pb age constraints from Iran on the magmatic evolution related to Neotethyan subduction and Zagros orogeny
This study reports zircon LA-ICPMS U–Pb ages of 50 igneous rock samples from the
Urumieh–Dokhtar magmatic arc (UDMA) and Sanandaj–Sirjan structural zone (SSZ) in Iran …
Urumieh–Dokhtar magmatic arc (UDMA) and Sanandaj–Sirjan structural zone (SSZ) in Iran …
The Neotethyan Sanandaj‐Sirjan zone of Iran as an archetype for passive margin‐arc transitions
Abstract The Sanandaj‐Sirjan zone of Iran is a northwest trending orogenic belt immediately
north of the Zagros suture, which represents the former position of the Neotethys Ocean. The …
north of the Zagros suture, which represents the former position of the Neotethys Ocean. The …
Cenozoic tectonic evolution of Asia: A preliminary synthesis
Asia has been a major testing ground for various competing models of continental
deformation due to its relatively well-understood plate boundary conditions in the Cenozoic …
deformation due to its relatively well-understood plate boundary conditions in the Cenozoic …
Granitic record of the assembly of the Asian continent
The Asian continent consists of many continental blocks that assembled during the
Phanerozoic, accompanied by widespread granitoids. By compiling a series of digital maps …
Phanerozoic, accompanied by widespread granitoids. By compiling a series of digital maps …
Retrodeforming the Arabia-Eurasia collision zone: Age of collision versus magnitude of continental subduction
Abstract The Arabia-Eurasia collision has been linked to global cooling, the slowing of
Africa, Mediterranean extension, the rifting of the Red Sea, an increase in exhumation and …
Africa, Mediterranean extension, the rifting of the Red Sea, an increase in exhumation and …